| 山西断陷盆地内强震的原地重复特点 |
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| 引用本文： | 武烈.山西断陷盆地内强震的原地重复特点[J].西北地震学报,1985,7(3):49-56. |
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| 作者姓名： | 武烈 |
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| 作者单位： | 山西省地震局 |
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| 摘 要： | 山西的一些断陷盆地是华北地震区内6级以上地震活动的重要场所。本文在详细研究每个6级以上地震的震中部位、烈度等震线特点、时间序列特征、发震构造走向后得出:在同一盆地内,6级以上地震原地重复发生,而且震级相近,时间间隔较短,发震构造走向正交或斜交,发震构造的类型也有所不同。
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| 收稿时间： | 1984/6/18 0:00:00 |
THE CHARACTERS OF THE REPETITION OF THE STRONG EARTHQUAKES IN THE SAME LOCATION OF SHANXI SUBSIDENCE BASIN |
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| Wu Lie.THE CHARACTERS OF THE REPETITION OF THE STRONG EARTHQUAKES IN THE SAME LOCATION OF SHANXI SUBSIDENCE BASIN[J].Northwestern Seismological Journal,1985,7(3):49-56. |
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| Authors: | Wu Lie |
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| Institution: | Seismolgical Bureau of Shanxi Province, China |
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| Abstract: | Shanxi subsidence basin is an important area in North China, where strong earthquakes(M=6.0)always visit. This paper deals with the location of epicenters of the earthquakes, the isoseismal lines, the temporal sequences and the tectonic strike of all the strong earthquakes(M=6.0)in this area.The following preliminary results can be done in this paper:In the same subsidence basin, there are earthqakes of M=6.0 which occur repeatedly in the same spot with approximate magnitude, short interval, oblique or normal strike and the different kinds of seismogenic structure. |
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